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The main objective of this research was to enhance the understanding of the inteÂ¬ractions of bentonite with iron in the near field of a HLW-repository. One target was to investigate natural Fe-rich bentonites as a possible analogue. Another topic was to recognize the mineralogical interaction of bentonite with iron powder simulating the contact of bentonite with steel containers (thermodynamic approach). An additional objective was to explore the idea that bentonites have a specific dissolution potential (kinetic approach). In order to take the thermodynamic approach, compacted MX80 bentonite and Friedland clay were used as starting materials for clay/iron interaction experiments in perÂ¬colation systems (Clay/Iron-ratio = 0.1). The natural processes were studied by examining a tropical weaÂ¬thering profile of serpentinizÂ¬ed diabase from the Thanh Hoa province of Vietnam. The kinetic approach was taken by investigating a series of well characterized bentonites, 9 from API-standard series, 12 from the BGR-collection and 4 others, all of them saturated with deionized water (liquid/solid-ratio = 10/1) and NaCl 1N solution (liquid/solid-ratio = 4/1) for 30 days, followed by exposing the soft gels to mechanical agitation by overhead shaking corresponding to two energy levels (20 rpm and 60 rpm). XRD and TEM â€“ EDX measurement were the major analytical techniques applied in this research, with FT-IR and XRF analyses as additional tools to characterizing the structure and composition of the smectites. Thermodynamic Approach MX80 bentonite and Friedland Clay clearly show that chemical and mineralogical changes have occured in the reaction products. They are exemplified by the neoformation of serpentine and chlorite in certain mixed layer phases. The smectite in the reaction products had also undergone changes especially in the constitution of the octahedral and tetrahedral sheets as well as in the interlayer space. These alterations were evident by the difference in key peak positions and ratios of XRD-patterns, and by TEM-investigations, as well as by different positions and intensities of FT-IR-bands of octahedral and tetrahedral features. The alteration was also seen in the bulk chemical composition data (XRF). MX80 bentonite and Friedland clay show various types and stages of alteration under different experimental conditions. The alteration can be described as â€śillitizationâ€ť in open reaction systems and â€śsmectitizationâ€ť in closed reaction systems. The degree of alteration was controlled by the degree of chemical activities (ion strength, Fe- & Si-activity, con-centration). Higher reactivities give higher degrees of dissolution and release of Si from clay minerals. The oxidation of native iron (Fe0 â†’ Fe2+) was recognized as the main driving force for dissolution, but also the oxidation of Fe2+ (Fe2+ â†’ Fe3+) appeared to reverse an open to a closed reaction system by increased Si-preÂ¬cipitation. The thermodynamic modelling of C/I-experiments by Mingliang Xie (GRS mbH) verified identified mineralogical alterations in the reaction products. Generally, the contact with metallic iron caused a strong increase in dissolution potential. The reason for this is the reducing potential of oxidation of iron which raised pH to become alkaline and increase dissolution of Si from clay particles. The mineralogical transformations recognized in the experiments, such as the neoformation of serpentine and chlorite phases, were also observed in the tropical weathering profile of serpentinized diabase. The wellknown fast development of Fe-rich montmorillonite in alteration of ultramafic rocks (e.g., Schnellmann, 1964) was also identified by mineralogical investigation of the weatherÂ¬ing profile. This confirms that smectitization is linked with higher Fe-activities also in nature. Fe2+ was present in this system and during oxidation acted as driving force for alteration. The reduction potential of Fe-oxidation caused an increase of pH into alkaline conditions. Kinetic Approach The hypothesis that smectite clays have a specific dissolution potential emanated from the study. This would mean that high amounts of Fe and Mg in the octahedral sheet can accelerate alteration in agreement to what was early proposed by Cicel & Novak (1976). The larger ion diameter of Fe and Mg in comparison with Al may well be responsible for a higher sheet stress, which would facilitate dissolution of smectites. The idea proposed Kaufhold & Dohrmann (2008) concerning a mechanism that makes Ca- and Mg-cations in the interlayer space stabilize quasicrystals is also supported by the present study. The performed investigation indicate which mechanisms that serve to protect smectites from undergoing alteration and which promote alteration. Stable smectites, i.e. those with a low specific dissolution potential, were called here â€śSleepersâ€ť, while fast reacting bentonites, which have a high specific dissolution potential, were termed â€śSprintersâ€ť. Smectites react with different rates of reaction in laboratory experiments. As said, each smectite sample has its specific potential for dissolution and this potential is controlled by the composition of both the octahedral sheets and the interlayer space. Increasing amounts of octahedral Fe and Mg compared to octahedral Al increase the specific dissolution potential. This potential is also affected by the ion radius, implying that the larger ion radius of Fe and Mg compared to Al increases the mechanical sheet stresses in the octahedral sheet. In summary, this means that, the investigations have confirmed the initial hypothesis concerning the impact of the composition of the octahedral sheet. It results primarily from the pH during the formation of the smectite clay and therefore serves as a geological fingerprint. The Al-Fe ratio in the octahedral sheet influences the stability of the interlayer: A) Aloct > 1.4 and Feoct > 0.2 (per (OH)2 O10) favour delamination of quasicrystals. The swelling pressure increases by a co-volume process between the delaminated layers wiht higher numbers of quasicrystals for Na-dominant population of the interlayer space (Laird, 2006). The microstructural components including both small and large particles and parts of them have a very small ability to move and undergo free rotation. Such Na-montmorillonites are consider as stable phases and have only a low specific dissolution potential. They are â€žSleepersâ€ś. B) Aloct > 1.4 and Feoct < 0.2 or Aloct < 1.4 and Feoct > 0.2 (per (OH)2 O10) promote demixing of monovalent and divalent interlayer cations (Laird, 2006). In the case of Ca and Mg-dominant interlayers, quasicrystal can break Na-bearing interlayers and help to maintain the quasicrystal structure. Such Ca and Mg-montÂ¬morillonites can be also be taken as â€žSleepersâ€ś because of their low specific dissolution potential. Depending on the octahedral composition, certain cations in the interÂ¬layer can stabilize bentonites against mineralogical changes. Montmorillonites stabilized by high concentration of Na-cations were classified as belonging to category A, while montmorillonites stabilized by high Ca, Mg-cations in the interlayer sheet were grouped in category B. The classification of a smecÂ¬tite into the categories A or B defined above can be best achieved by IR analyses that yield useful chemical information concerning the composition of the octahedral sheets. Smectites with Na as stabilizing interlayer cation (group A) have shown Î´AlAlOH-bands with increasing wavenumbers for increasing octahedral Al in FT-IR spectra. The other reaction type of smectite, with Ca, Mg-cations in the interlayers (group B), is characterized by a decreasing octahedral Al-amount for increasing wavenumbers of Î´AlAlOH-bands in such spectra. Also the FT-IR Î´AlFeOH-bands are different in the two reaction types of smectite. Increasing octahedral Fe-amounts were mirrored by decreasing wavenumbers of Î´AlFeOH-bands. However, smectites of group B do contain higher Fe-amounts for the same wavenumber than smectites of group A. Expected alteration of bentonite close and far from a steel canister In the early interaction of smectite-rich clay â€“ the â€śbufferâ€ť - and steel, the system behaves as being chemically closed. Within the clay barrier, Si will be dissolved from clay mineral particles in accordance with its specific disÂ¬solution potential. The dissolved Si can stay by contributing neoformation of montÂ¬morillonite layers in mixed layer phases. The interlayer charge decreases by substitution of Mg by Al, which leads to an increase in the swelling pressure. Also minor Si-precipitation may occur if not all the dissolved Si is used up by the neoformed montmorillonite layers. Such precipitation of Si will cause cementation of some quasicrystals and lead to a reduction in porosity. Enhanced temperature and additional Fe-activity, representing an increased reduction potential, increases notably the amount of dissolved Si at the interface between bentonite and steel canister, and as a consequence there will be significant precipitation of Si. The resulting cementation of quasicrystals is acÂ¬comÂ¬panied also by their collapse which induces broadening of pores. This caused the channel-like migration of infiltrating solutions and switches the system into an open one. Thermodynamic predictions indicate that â€śilliteâ€ť will be generated close to the steel canister (via â€śillitizationâ€ť) and kaolinite or pyrophyllite to be formed farther away (via smectitization). The â€śillitizationâ€ť process results in higher interlayer charges and lower swelling pressures. In contrast, the formation of smectite reduces interlayer charges and promotes higher swelling pressures. At the end of the thermodynamic evolution, the swelling pressure will drop also far from the canister because kaolinite and pyrophyllite are non-swelling minerals. In both cases, the applications of so-called â€śSleeperâ€ť-bentonites are required to slow the reaction progress. For designers of the engineered barriers in a repository, i.e. the canister and the â€śbufferâ€ť clay, some basic rules are recommend on the basis of the present study. Thus, the presence of native Fe or Fe2+-cations in the clay or in accessory minerals in it, or emanating from the canisters, will speed up the reaction process and make it extensive. Likewise, use of Fe-poor â€śbufferâ€ť clay, representing â€śSleepersâ€ť-type are suitable for slowing down the reaction. Copper as canister material, and very dense Na-rich montmorillonite of group A as â€śbufferâ€ť seem to be ideal rather than steel/iron and less dense Ca-saturated clay.